Foraminifera taxon details

Leptohalysis Loeblich & Tappan, 1984

556143  (urn:lsid:marinespecies.org:taxname:556143)

accepted
Genus
Reophax catella Höglund, 1947 accepted as Leptohalysis catella (Höglund, 1947) (type by original designation)
Leptohyalis · unaccepted (Incorrect subsequent spelling of...)  
Incorrect subsequent spelling of Leptohalysis

Ordering

  • Alphabetically
  • By status

Children Display

marine, brackish, fresh, terrestrial
recent only
feminine
Loeblich, A. R.; Tappan, H. (1984). Some new proteinaceous and agglutinated genera of Foraminiferida. <em>Journal of Paleontology.</em> 58: 1158-1163.
page(s): p. 1160; note: Genus is feminine [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Leptohalysis Loeblich & Tappan, 1984. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=556143 on 2024-03-29
Date
action
by
2010-12-20 09:45:26Z
created
2010-12-22 06:22:46Z
changed
2013-08-17 09:28:49Z
changed
2014-02-27 08:48:43Z
changed
2017-09-25 14:20:39Z
changed
2019-06-23 15:32:30Z
changed

original description Loeblich, A. R.; Tappan, H. (1984). Some new proteinaceous and agglutinated genera of Foraminiferida. <em>Journal of Paleontology.</em> 58: 1158-1163.
page(s): p. 1160; note: Genus is feminine [details]  Available for editors  PDF available [request] 

context source (Deepsea) Kitazato H., Uematsui K., Todo Y., Gooday A.J. (2009). New species of Leptohalysis (Rhizaria, Foraminifera) from an extreme hadal site in the Western Pacific Ocean. <em>Zootaxa.</em> 2059: 23-32., available online at http://www.mapress.com/zootaxa/2009/f/z02059p032f.pdf [details]  Available for editors  PDF available [request] 
From editor or global species database
Diagnosis Test uniserial and rectilinear, globular proloculus followed by an elongate series of gradually enlarging and distally tapering flaskshaped chambers with blunt lower margin; wall very thin, delicate, and flexible, consisting of a single layer of minute quartz and mica grains agglutinated on a proteinaceous base, early stage may have foreign particles widely spaced, later with adjacent grains abutting; aperture a simple terminal opening, may be flush with the surface or slightly produced with a phialine neck, and may have more than one layer of grains immediately around the opening. Holocene; N. Atlantic: England at20m to46m; Norway from 150m to200m; Sweden from 20 m to 515 m. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]